Abstract The North Atlantic, extending from the Charlie Gibbs Fracture Zone to the north
Norway-Greenland-Svalbard margins, is regarded as both a classic case of structural …

The stunningly increased resolution of the deep crustal levels in recent industrial seismic
profiles acquired along most of the world's rifted margins leads to the unraveling of an …

Abstract The Norwegian Margin formed in response to early Cenozoic continental breakup
and subsequent opening of the Norwegian-Greenland Sea. There is a welldefined margin …

In the preceding chapters we have included only a few regional examples and case studies
because of space limitations. The present chapter will, however, provide some examples …

The Barents Shelf, stretching from the Arctic Ocean to the coasts of northern Norway and
Russia, and from the Norwegian–Greenland Sea to Novaya Zemlya, covers two major …

Palaeogeographic and tectono-stratigraphic considerations in the greater Barents Sea show
that the distribution of reservoirs and hydrocarbon source rocks from the Late Palaeozoic to …

A sequence stratigraphic framework of the Triassic on the Norwegian Barents shelf is
presented. The Triassic succession was subdivided into five second-order sequences based …

Deep seismic data from the Hatton-Rockall region, the mid-Norway margin and the SW
Barents Sea provide images of the crustal structure that make it possible to estimate the …

The world's 877 giant oil and gas fields are those with 500 million bbl of ultimately
recoverable oil or gas equivalent. Remarkably, almost all of these 877 giant fields, which by …

ABSTRACT The Laurentian, Baltic, and Siberian blocks of the modern circum-Arctic were
scattered across a broad area between 10 S and 30 N during the Late Ordovician. Closure …